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34<br />

<strong>be</strong>en ~nterpreted ar a rub-flwr ddnage system rdwiched <strong>be</strong>tween the original eanhen<br />

floor (Event 36) and Uls wcond eanhen flex (Event 4). It will k descri<strong>be</strong>d in detail in<br />

Chapter 2.<br />

Event 5<br />

The parent subsoxl <strong>be</strong>neath the cultural mam wn designated ar Event 5. It consisted <strong>of</strong><br />

two types <strong>of</strong> roil matrix. In pluces. it war ehterired as a reddish-bmwn sandy gravel<br />

while in other mas. notably along the mkrn mwt portion <strong>of</strong> the rite. it had a greyish<br />

white sandy clay matrix. A small num<strong>be</strong>r <strong>of</strong> wventeentheentury yrifafe was recovered<br />

from this stratum. nKy had likely fwnd thur way into this orheruise sterile s mm<br />

through the heaving action <strong>of</strong> U. annual cycle d freeze-thaw activity.<br />

Event 6<br />

This dcslgnation was arslgned to a fill dcpit diseovercd in n b arn pit (Feaure 3.<br />

Figure 191 neu t k south side <strong>of</strong> the house. The roil matrix consisIed <strong>of</strong> what u ppad to<br />

<strong>be</strong> redeprited grey-green or eream-mlwred randy clay rubroil. A small num<strong>be</strong>r af<br />

anihar was recovered fmm chis pit 811, lhe date range <strong>of</strong> which war unurually bmd for<br />

such r spatially limited depit. my have t en dated from the rcwntrmth to the late<br />

eighteenth and possibly even early nirrtrrnth-xnwien.

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